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Results:

• 41. VI_2015_009

  by rescaling a dimensionless regional flood frequency distribution or growth curve, qR(D;T ), com- mon to all sites of the homogeneous region, with the so-called index flood, µi(D), of the target site: bQi(D;T ) = µi(D)qR(D;T ); (1) where bQi(D;T ) is the estimated flood quantile, i.e. the T -year flood peak discharge averaged over duration D, at site i. The regional growth curve, qR(D;T /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 42. Publications 2014

  on the combined use of a hydrological model and an analogue method Philippe Crochet 68 2,8 2014-005 Evaluation of HARMONIE reanalyses of surface air temperature and wind speed over Iceland Nikolai Nawri 31 12 2014-001 Flood frequency estimation for ungauged catchments in Iceland by combined hydrological modeling and regional frequency analysis Philippe Crochet & Tinna /about-imo/publications/2014/

• 43. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 44. VI_2020_004

  ....................................................................................... 99 APPENDIX I. Daily tephra dispersal simulation .................................................................... 102 APPENDIX II. HEKLA 1980 – The likelihood of receiving tephra at different locations .... 104 APPENDIX III. KATLA 1918 – The likelihood of receiving tephra at different locations ... 107 APPENDIX IV. ÖRÆFAJÖKULL 1362 /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 45. VI2010-006_web

  5.6 Hafnarstræti 23–89 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 34 5.7 Grófargil . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 36 5.8 Gleráreyrar og farvegur Brunnár . . . . . . . . . . . . . . . . . . . . . . . . . 36 6 Niðurstaða 37 7 Heimildir 38 Viðaukar I Tæknileg hugtök og skilgreiningar 41 II Langsnið brauta 43 III Kort 49 5 6 1 /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 46. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  mover’s payoff, while mover 2’s payoff is greater than or equal to the first mover’s payoff. The payoff function is that of the basic public good game. The marginal return from the public good is a ∈ [0,1], and each agent’s initial endowment is E. The payoff function Rik of agent i as mover k, k = 1 for the first mover and k = 2 for the second mover, is defined as follows: Rik =E − xik + a (xik /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 47. Group-1_Scenarios-for-AWM

  example can be given by the low cost still flood risk adaptation by implementing early warning system. But there is one more suggestion dfor stakeholders to restrict infrastructure in the cities of Horsens. Fiva PhD Courses : Adaptive management in relation to climate change (august 22 2011 - august 26 2011) 2 / 3 R es e a r c h Flood f r equenc y a n d i n t ensi t y c o m m un i c a t /media/loftslag/Group-1_Scenarios-for-AWM.pdf

• 48. ces_risk_flyer

  a comprehensive assessment of the impact of climate change on renewable energy resources in the Nordic area including hydropower, wind power, bio‐fuels and solar energy. M i bj i f h CES P j An increase of uncertainty about the future of renewable resources under climate change is a key issue for the energy sector. Some renewable energy resources are likely to increase their productivity /media/ces/ces_risk_flyer.pdf

• 49. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  1 PhD Workshop preceding Adaptation Research Conference – 27 & 28 August, Helsinki Climate change adaptation - Analysis, Planning and Implementation Programme Venue: Rantapuisto, Ramsinniementie 14, FIN-00980 HELSINKI directions for travel can be found at the conference web site http://www.nordicadaptation2012.net/ Informal start at 26 August On Sunday evening 8pm an informal get /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 50. esa_flyer_new

  EA Analyse A/S and Optensys Energianalys will forecast energy system variables, while SINTEF Energy Research will make assumptions for the energy system in different cases, include new inputs in the EMPS model and carry out simulations. Cl i ma t e Sc e nar i os G ro u p R i s ø St o c h as t i c v a r i a b l e s Clima t e s c e n a r i o NV E S M H I FE I N o r w a y S w e d e n F inla n /media/ces/esa_flyer_new.pdf